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Journal articles on the topic 'Magnetotelluric studies'

Author: Grafiati

Published: 6 September 2023

Last updated: 31 July 2025

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1

Chen, Kai, Sheng Jin, and Ming Deng. "Multifunction waveform generator for EM receiver testing." Geoscientific Instrumentation, Methods and Data Systems 7, no. 1 (2018): 11–19. http://dx.doi.org/10.5194/gi-7-11-2018.

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Abstract. In many electromagnetic (EM) methods – such as magnetotelluric, spectral-induced polarization (SIP), time-domain-induced polarization (TDIP), and controlled-source audio magnetotelluric (CSAMT) methods – it is important to evaluate and test the EM receivers during their development stage. To assess the performance of the developed EM receivers, controlled synthetic data that simulate the observed signals in different modes are required. In CSAMT and SIP mode testing, the waveform generator should use the GPS time as the reference for repeating schedule. Based on our testing, the freq

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2

Gokarn, S. G., C. K. Rao, B. P. Singh, and P. N. Nayak. "Magnetotelluric studies across the Kurduwadi gravity feature." Physics of the Earth and Planetary Interiors 72, no. 1-2 (1992): 58–67. http://dx.doi.org/10.1016/0031-9201(92)90049-2.

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Unsworth, Martyn. "Magnetotelluric Studies of Active Continent–Continent Collisions." Surveys in Geophysics 31, no. 2 (2009): 137–61. http://dx.doi.org/10.1007/s10712-009-9086-y.

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Young, Charles T., John R. Booker, Ricardo Fernandez, et al. "Verification of five magnetotelluric systems in the mini‐EMSLAB experiment." GEOPHYSICS 53, no. 4 (1988): 553–57. http://dx.doi.org/10.1190/1.1442487.

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Given the degree of complexity of modern magnetotelluric (MT) instrumentation, comparison of the total performance for two or more systems is an important verification test. This paper compares the processed data from five MT systems which were designed and constructed separately, and which employ different electrode types, electrode separations, magnetometers, and methods of signal processing. The comparison shows that there is a high degree of agreement among the data from the different systems. The study also demonstrates the compatibility and reliability of the MT systems employed as part

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5

Bayartogtokh, Enkhzul, and Batmagnai Erdenechimeg. "The relationship between geological features and phase tensor: examples from Mogod an Tsenker study areas." Mongolian Journal of Astronomy and Geophysics 11, no. 1 (2024): 73–83. https://doi.org/10.5564/mjag.v11i1.4191.

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The magnetotelluric phase tensor contains information about the directionality and dimensionality of the study region’s geo-electrical structure. In this context, the phase tensor controls geological faults or fractured zones and homogeneities of the lithology. Although the phase tensor is commonly used for magnetotelluric analysis, it is still poorly introduced in Mongolian case studies. Therefore, this paper introduces the theoretical concepts of the phase tensors and their applications in the Tsenkher and Mogod geothermal regions. For this study, we used magnetotelluric data sets from the p

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Lantu, Syamsuddin, and A. Hardianti Yunus. "KARAKTERISASI ZONA RESERVOAR CEKUNGAN BULA MALUKU DENGAN METODE ELEKTROMAGNETIK MAGNETOTELLURIK." JURNAL GEOCELEBES 1, no. 1 (2017): 23. http://dx.doi.org/10.20956/geocelebes.v1i1.1777.

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AbstrakTelah dilakukan penelitian dengan metode elaktromagnetik tellurik untuk karakterisasi zona reservoir hidrokarbon di daerah Bula Kabupaten Seram bagian timur, propinsi Maluku. Ditinjau dari tektonik lempeng , daerah ini merupakan cekungan sedimen yang kaya akan hidrokarbon. Metode yang digunakan untuk identifikasi potensi cekungan sedimen tersebut digunakan metode elektromagnetik magnetotellurik untukkarakterisasi sifat listrik sedimen yang terdapat pada cekungan teresbut. Tujuan utama penelitian adalah identifikasi zona reservoar potensial didaerah ini. Analisis dan interpretasi pengola

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Chen, C. S., F. Hsieh, D. Zuo, J. Li, Lin Lin, and G. Xie. "Magnetotelluric Modelling and Inversion For Earthquake Studies in Taiwan." ASEG Extended Abstracts 2003, no. 1 (2003): 1–5. http://dx.doi.org/10.1071/aseg2003_3demab003.

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8

Gokarn, S. G., Gautam Gupta, Shipra Dutta, and Nitu Hazarika. "Geoelectric structure in the Andaman Islands using magnetotelluric studies." Earth, Planets and Space 58, no. 2 (2006): 259–64. http://dx.doi.org/10.1186/bf03353386.

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9

Gokarn, S. G., C. K. Rao, and Gautam Gupta. "Crustal structure in the Siwalik Himalayas using magnetotelluric studies." Earth, Planets and Space 54, no. 1 (2002): 19–30. http://dx.doi.org/10.1186/bf03352418.

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10

Gokarn, S. G., C. K. Rao, Gautam Gupta, B. P. Singh, and M. Yamashita. "Deep crustal structure in central India using magnetotelluric studies." Geophysical Journal International 144, no. 3 (2001): 685–94. http://dx.doi.org/10.1046/j.1365-246x.2001.01355.x.

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11

de Lugão, Patricia Pastana, Emanuele Francesco LaTerra, Berthold Kriegshäuser, and Sergio L. Fontes. "Magnetotelluric studies of the Caldas Novas geothermal reservoir, Brazil." Journal of Applied Geophysics 49, no. 1-2 (2002): 33–46. http://dx.doi.org/10.1016/s0926-9851(01)00097-0.

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12

Pospeeva, E. V., and V. V. Potapov. "The results of magnetotelluric studies on the profile of the Kuray depression – lake Teletskoye." IOP Conference Series: Earth and Environmental Science 929, no. 1 (2021): 012026. http://dx.doi.org/10.1088/1755-1315/929/1/012026.

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Abstract The results of magnetotelluric studies (MTS) conducted in the western part of the Mountainous Altai region on the profile of the Kurai depression – lake Teletskoye are presented. The profile intersects two large tectonic units – the Mountainous Altai and Teletskaya, bounded by regional tectonic suturs of the Teletsko-Bashkausskiy, Northern Sayans, Shapshalskiy and other faults. The obtained data indicate a fairly fractional recent block divisibility of the Earth’s crust of the Mountainous Altai territory. It is shown that according to the characteristics of the electrical resistivity

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Hill, Graham J. "On the Use of Electromagnetics for Earth Imaging of the Polar Regions." Surveys in Geophysics 41, no. 1 (2019): 5–45. http://dx.doi.org/10.1007/s10712-019-09570-8.

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Abstract The polar regions are host to fundamental unresolved challenges in Earth studies. The nature of these regions necessitates the use of geophysics to address these issues, with electromagnetic and, in particular, magnetotelluric studies finding favour and being applied over a number of different scales. The unique geography and climatic conditions of the polar regions means collecting magnetotelluric data at high latitudes, which presents challenges not typically encountered and may result in significant measurement errors. (1) The very high contact resistance between electrodes and the

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14

Mekkawi, M., and A. Saleh. "Case studies of magnetotelluric method applied to mapping active faults." Acta Geodaetica et Geophysica Hungarica 42, no. 4 (2007): 383–97. http://dx.doi.org/10.1556/ageod.42.2007.4.2.

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15

Bubnov, Valeriy P., Andrey G. Yakovlev, Elena D. Aleksanova, Denis V. Yakovlev, Mark N. Berdichevsky, and Pavel Yu Pushkarev. "Magnetotelluric studies of the East-European Craton and adjacent regions." Acta Geophysica 55, no. 2 (2006): 154–68. http://dx.doi.org/10.2478/s11600-006-0034-7.

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16

Belyavsky, V. V. "The use of invariant MTS curves in deep magnetotelluric studies." Izvestiya, Physics of the Solid Earth 43, no. 3 (2007): 237–44. http://dx.doi.org/10.1134/s1069351307030081.

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17

Wu, Chaofeng, Xiangyun Hu, and Guiling Wang. "Magnetotelluric studies in the Zhangzhou Basin geothermal zone, southeastern China." Acta Geologica Sinica - English Edition 93, S1 (2019): 277. http://dx.doi.org/10.1111/1755-6724.14088.

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18

Mohan, Kapil, B. K. Rastogi, and Peush Chaudhary. "Magnetotelluric studies in the epicenter zone of 2001, Bhuj earthquake." Journal of Asian Earth Sciences 98 (February 2015): 75–84. http://dx.doi.org/10.1016/j.jseaes.2014.10.019.

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19

Lagios, E., A. Tzanis, N. Delibasis, J. Drakopoulos, and G. K. J. Dawes. "Geothermal exploration of kos island, Greece: Magnetotelluric and microseismicity studies." Geothermics 23, no. 3 (1994): 267–81. http://dx.doi.org/10.1016/0375-6505(94)90004-3.

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20

Ghanbarifar, Saeed, Seyed Masoud Ghiasi, Seyed Hossein Hosseini, Maysam Abedi, Behrooz Oskooi, and Maxim Yu Smirnov. "Geoelectrical image of the Sabalan geothermal reservoir from magnetotelluric studies." Journal of Applied Geophysics 224 (May 2024): 105359. http://dx.doi.org/10.1016/j.jappgeo.2024.105359.

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21

Starzhinskii, S. S. "Analysis of Magnetotelluric Response Functions at the Cam Thuy Site, Northern Vietnam." Физика земли, no. 2 (May 23, 2024): 131–45. http://dx.doi.org/10.31857/s0002333724020102.

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During magnetotelluric studies in North Vietnam, an effect where the impedance phases Zxy and Zyx simultaneously left their quadrants was detected at one of the sounding sites, CTH, in the Cam Thuy District, Thanh Hoa Province. Investigation of this phenomenon has shown that it is accompanied by negative (bottom-up directed) components of the Umov–Poynting vector of electromagnetic energy flux density in the entire range of the recorded periods of magnetotelluric variations. This direction of the energy flux remains unchanged when the initial coordinate system is rotated by angles of 45° and 6

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22

Boerner, D. E., J. A. Wright, J. G. Thurlow, and L. E. Reed. "Tensor CSAMT studies at the Buchans Mine in central Newfoundland." GEOPHYSICS 58, no. 1 (1993): 12–19. http://dx.doi.org/10.1190/1.1443342.

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A novel application of the tensor controlled source audio‐magnetotelluric (CSAMT) method was part of a multidisciplinary geophysical study of an existing mine site at Buchans, Newfoundland. The orthogonal components of the horizontal electromagnetic fields used for magnetotelluric and CSAMT interpretation of the earth’s conductivity structure were found to be inappropriate at Buchans because of strong scattering in the electric fields. Instead, the length of the major axes of the electric and magnetic field polarization ellipses and the vertical magnetic field were used as data. The data from

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Gupta, Gautam, C. K. Rao, and S. G. Gokarn. "Deep Geoelectric Structure in the Rohtak Region Using the Magnetotelluric Studies." Journal Geological Society of India 50, no. 6 (1997): 697–708. http://dx.doi.org/10.17491/jgsi/1997/500605.

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Abstract Magnetotelluric studies conducted in the seismically active regions around Rohtak over two linear profiles showed a predominantly two dimensional behaviour with major and minor rotation directions along the E-W and N-S respectively, indicative of strong influence of an approximately N-S arfgned conductive feature. The geoelectric structure indicates a 25m thick surface layer with a resistivity of 1.4 ohm-m corresponding to the alluvium. The thickness of the second (30 ohm-m) and third (1.2 ohm-m) layers were 50m and 150m respectively. These are interpreted to be due to the Siwalik sed

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24

Parr, R. S., and V. R. S. Hutton. "Magnetotelluric studies in and adjacent to the Northumberland Basin, Northern England." Physics of the Earth and Planetary Interiors 81, no. 1-4 (1993): 43–66. http://dx.doi.org/10.1016/0031-9201(93)90123-q.

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25

Wei, W. "Detection of Widespread Fluids in the Tibetan Crust by Magnetotelluric Studies." Science 292, no. 5517 (2001): 716–19. http://dx.doi.org/10.1126/science.1010580.

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26

Pospeeva, E. V., and V. V. Potapov. "Deep Structure of the Junction Zones of the Chuya Tectonic Depression and Its Mountainous Frame in Gorny Altai according to Magnetotelluric Studies." Russian Geology and Geophysics 62, no. 4 (2021): 474–85. http://dx.doi.org/10.2113/rgg20194078.

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Abstract ––Results of magnetotelluric studies (MTS) carried out along the SW–NE and W–E profiles across the Chuya depression are used to demonstrate the deep geoelectric structure of its internal field and the zones of transition to the northern (Kurai Ridge) and southern (South Chuya Ridge) mountainous frames. The Chuya depression is an area with small-block structure, with its axial part comprised of the thinnest sedimentary deposits (450–650 m). The key sites of the zones of transition from this depression to the Kurai and the South Chuya ridges manifest a complete geoelectric section of se

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27

Hasanalizadeh Kolagari, Maedeh, and Ali Nejati Kalateh. "Focused and Smooth Inversion2D modelling of Magnetotelluric data from the Sabalan Geothermal Field in Northwestern Iran." Annals of Geophysics 67, no. 1 (2024): GM106. http://dx.doi.org/10.4401/ag-8973.

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Magnetotelluric measurements from the Sabalan geothermal field in northwestern Iran have provided clear indications of geothermal reservoirs. This study aimed to identify shallow and deeper conductivity anomalies associated with geothermal systems in the Sabalan area. The magnetotelluric method is widely used for exploring subsurface resources, as it is suitable for detecting subsurface anomalies at significant depths. Based on modeling results, thick conductive layer was found near the surface of the Moil Valley area, where two reservoirs are embedded. The main reservoir, located on the west

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28

Belyavsky, V. V. "Geoelectric Model of the Central Part of the Northern Caucasus and Its Fluid Saturation." Физика земли 2023, no. 4 (2023): 75–95. http://dx.doi.org/10.31857/s0002333723040014.

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A series of magnetotelluric and seismic studies have been carried out on profiles covering more than two thousand kilometers within the North Caucasus region. The earlier interpretation of the magnetotelluric observations by means of one– and two–dimensional inversion and three–dimensional mathematical modeling software has helped to construct a series of sections and models which are viewed as test and starting ones for the construction of a three–dimensional geoelectric model of the region. The test models have been used to test how well the software for three–dimensional inversion of the im

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Piña-Varas, Perla, Juanjo Ledo, Pilar Queralt, Alex Marcuello, Gemma Mitjanas, and David Martínez Van Dorth. "Magnetotelluric applied to deep geothermal exploration: Canary Islands." BOLETÍN GEOLÓGICO Y MINERO 134, no. 3 (2023): 49–58. http://dx.doi.org/10.21701/bolgeomin/134.3/004.

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There is currently a growing interest in geothermal energy. Geothermal energy for electricity generation usually corresponds to deep reservoirs, located deeper than one kilometer. This will condition the geophysical methods to be used during the exploration of the geothermal system, being magnetotelluric (MT) the only electromagnetic method capable of reaching such depths. Commonly used in geothermal exploration, this method will provide information on the electrical resistivity distribution of the subsurface, and therefore will allow characterizing the main components of the system. This is t

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Kong, Wenxin, Changhong Lin, Handong Tan, Miao Peng, Tuo Tong, and Mao Wang. "The Effects of 3D Electrical Anisotropy on Magnetotelluric Responses: Synthetic Case Studies." Journal of Environmental and Engineering Geophysics 23, no. 1 (2018): 61–75. http://dx.doi.org/10.2113/jeeg23.1.61.

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Using the staggered-grid finite difference method, a numerical modeling algorithm for a 3D arbitrary anisotropic Earth is implemented based on magnetotelluric (MT) theory. After the validation of this algorithm and comparison with predecessors, it was applied to several qualitative and quantitative analyses containing electrical anisotropy and a simple 3D prism model. It was found that anisotropic parameters for ρ 1 , ρ 2 , and ρ 3 play almost the same role in affecting 3D MT responses as in 1D and 2D without considering three Euler's angles α S , α D , and α L . Significant differences appear

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Begum, S. Kareemunnisa, and T. Harinarayana. "Basement Configuration from Magnetotelluric Studies in Bhuj Earthquake Epicentral Zone, Gujarat, India." Open Journal of Earthquake Research 05, no. 03 (2016): 177–88. http://dx.doi.org/10.4236/ojer.2016.53015.

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Patro, Prasanta K., and T. Harinarayana. "Deep geoelectric structure of the Sikkim Himalayas (NE India) using magnetotelluric studies." Physics of the Earth and Planetary Interiors 173, no. 1-2 (2009): 171–76. http://dx.doi.org/10.1016/j.pepi.2008.10.011.

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Beamish, D., and J. M. Travassos. "Magnetotelluric studies from two contrasting Brazilian basins: a reassessment of old data." Physics of the Earth and Planetary Interiors 81, no. 1-4 (1993): 261–76. http://dx.doi.org/10.1016/0031-9201(93)90135-v.

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Patro, Prasanta K. "Magnetotelluric Studies for Hydrocarbon and Geothermal Resources: Examples from the Asian Region." Surveys in Geophysics 38, no. 5 (2017): 1005–41. http://dx.doi.org/10.1007/s10712-017-9439-x.

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35

Türkoğlu, Erşan, Martyn Unsworth, and Dinu Pana. "Deep electrical structure of northern Alberta (Canada): implications for diamond exploration." Canadian Journal of Earth Sciences 46, no. 2 (2009): 139–54. http://dx.doi.org/10.1139/e09-009.

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Geophysical studies of upper mantle structure can provide constraints on diamond formation. Teleseismic and magnetotelluric data can be used in diamond exploration by mapping the depth of the lithosphere–asthenosphere boundary. Studies in the central Slave Craton and at Fort-à-la-Corne have detected conductors in the lithospheric mantle close to, or beneath, diamondiferous kimberlites. Graphite can potentially explain the enhanced conductivity and may imply the presence of diamonds at greater depth. Petrologic arguments suggest that the shallow lithospheric mantle may be too oxidized to contai

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Pospeeva, Elena, and Vladimir Potapov. "DEEP STRUCTURE OF SOUTH-EASTERN PART OF THE WEST SIBIRIAN PLATE AND IN THE SALAIR ACCORDING TO MAGNETOTELLURIC SOUNDINGS." Interexpo GEO-Siberia 2, no. 2 (2019): 80–86. http://dx.doi.org/10.33764/2618-981x-2019-2-2-80-86.

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The first results of magnetotelluric studies carried out on the profile of v. Talmenka – Leninsk-Kuznetsky (South-Eastern part of the West Siberian plate and Salair) are considered, the main features of the distribution of deep electrical conductivity in the two main geological structures of the study area: the South-Eastern part of the West Siberian plate and the Salair zone are shown.

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García, Xavier, and Alan G. Jones. "A new methodology for the acquisition and processing of audio-magnetotelluric (AMT) data in the AMT dead band." GEOPHYSICS 70, no. 5 (2005): G119—G126. http://dx.doi.org/10.1190/1.2073889.

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Distant lightning activity, the natural energy source for the audio-magnetotelluric (AMT) method, has a signal minimum between 1 and 5 kHz, the so-called AMT dead band. The energy in this band exhibits both diurnal and annual variation; magnetic-field amplitudes during the daytime are often well below the noise levels of existing sensors (coil magnetometers), thus reducing the effectiveness of the method for quantitative high-resolution studies of near-surface targets. To overcome this deficiency, we propose a hybrid acquisition and processing methodology based on combining the telluric-tellur

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Pospeeva, E. V., F. I. Zhimulev, I. S. Novikov, and V. V. Potapov. "The deep structure of the Salair fold-cover structure according to magnetotelluric studies." IOP Conference Series: Earth and Environmental Science 929, no. 1 (2021): 012027. http://dx.doi.org/10.1088/1755-1315/929/1/012027.

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Abstract The results of magnetotelluric studies (MTS) performed within the Salair cover-folded structure on two profiles are considered: the Zabrodino village – the Rodnikovy village (1) and the Smaznevo village – the Kotino village (2). The profiles are oriented crosswise along the main structures and intersect Salair and the western part of the Kuznetskiy trough. The analysis of the obtained data showed that a subhorizontal underlying conducting zone is distinguished in the Earth’s crust of the Salair fold-cover structure, such zone is typical for intracontinental orogens. The zone is consid

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Rao, C. K., S. G. Gokarn, and B. P. Singh. "Upper Crustal Structure in the Torni-Purnad Region, Central India Using Magnetotelluric Studies." Journal of geomagnetism and geoelectricity 47, no. 4 (1995): 411–20. http://dx.doi.org/10.5636/jgg.47.411.

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Bastani, Mehrdad, Alireza Malehmir, and Alexandros Savvaidis. "Combined use of controlled-source and radio-magnetotelluric methods for near surface studies." ASEG Extended Abstracts 2015, no. 1 (2015): 1–4. http://dx.doi.org/10.1071/aseg2015ab255.

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CHEN, Chutong, Keying ZHU, Binbin LYU, et al. "Tectonic Evolution and Lithospheric Structure of the Beishan Orogen: Insights from Magnetotelluric Studies." Acta Geologica Sinica - English Edition 98, S1 (2024): 6–9. http://dx.doi.org/10.1111/1755-6724.15223.

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Kulikov, V. A., Iv M. Varentsov, P. V. Ivanov, et al. "Findings from Deep Magnetotelluric Studies in the Sloboda Geodynamic Intersection (East European Platform)." Russian Journal of Pacific Geology 18, S1 (2024): S1—S14. http://dx.doi.org/10.1134/s1819714024700167.

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Harinarayana, T., K. K. Abdul Azeez, K. Naganjaneyulu, et al. "Magnetotelluric studies in Puga valley geothermal field, NW Himalaya, Jammu and Kashmir, India." Journal of Volcanology and Geothermal Research 138, no. 3-4 (2004): 405–24. http://dx.doi.org/10.1016/j.jvolgeores.2004.07.011.

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Gupta, Gautam, S. G. Gokarn, and B. P. Singh. "Thickness of the Siwalik sediments in the Mohand-Ramnagar region using magnetotelluric studies." Physics of the Earth and Planetary Interiors 83, no. 3-4 (1994): 217–24. http://dx.doi.org/10.1016/0031-9201(94)90090-6.

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45

Harinarayana, T., K. Naganjaneyulu, and B. P. K. Patro. "Detection of a collision zone in south Indian shield region from magnetotelluric studies." Gondwana Research 10, no. 1-2 (2006): 48–56. http://dx.doi.org/10.1016/j.gr.2005.12.006.

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Patro, Prasanta K., and S. Dhamodharan. "An Overview of Magnetotelluric Studies in the Seismogenic Zones of the Indian Subcontinent." Journal Of The Geological Society Of India 101, no. 6 (2025): 931–36. https://doi.org/10.17491/jgsi/2025/174186.

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ABSTRACT Diverse tectonic settings of the Indian subcontinent necessitate continuous monitoring and the application of advanced geophysical techniques to understand seismogenic processes. The magnetotelluric (MT) method, a key geophysical method for imaging crust-to-mantle structures, analyses electrical resistivity variations to identify fluid-rich fault zones, subduction interfaces, and seismo-electromagnetic signals. Here, we summarize MT investigations in the seismogenic zones across the Indian subcontinent, providing insights into fault dynamics and seismic activity. For instance, in inte

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Stewart, Ian C. F., Thomas C. Connally, and Jeffrey H. Copley. "Stratigraphic Interpretation of Magnetotelluric Data in Central Saudi Arabia." GeoArabia 1, no. 1 (1996): 52–63. http://dx.doi.org/10.2113/geoarabia010152.

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ABSTRACT The pre-Khuff interval of the Paleozoic sediments in central Arabia is poorly defined by conventional seismic techniques, although this layer has significant potential for hydrocarbon exploration. Model studies indicated that magnetotelluric methods could outline the regional changes expected in the pre-Khuff in the area, which are largely dependent on the topography of the Precambrian basement. The Hercynian orogenic event created an extensive block-faulted terrane of half-grabens and horsts. The Hercynian structural relief was infilled in the Permo-Carboniferous and faulting reactiv

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Clowes, Ron M. "Initiation, development, and benefits of Lithoprobe — shaping the direction of Earth science research in Canada and beyondThis article is one of a series of papers published in this Special Issue on the theme Lithoprobe — parameters, processes, and the evolution of a continent.Lithoprobe Contribution 1480." Canadian Journal of Earth Sciences 47, no. 4 (2010): 291–314. http://dx.doi.org/10.1139/e09-074.

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Lithoprobe is Canada’s national, collaborative, multidisciplinary, Earth science research project established to develop a comprehensive understanding of the evolution of northern North America. It is regarded internationally as one of the most successful national geoscience projects ever undertaken. Part of Lithoprobe’s success derives from its history and organizational structure. A one-year Phase I program (1984–1985) was highly successful. Phases II to V carried the project forward until 2005, when funding terminated. Lithoprobe was organized as a decentralized research network of multidis

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Prystai, A. M., and V. O. Pronenko. "Improving of electrical channels for magnetotelluric sounding instrumentation." Geoscientific Instrumentation, Methods and Data Systems 4, no. 2 (2015): 149–54. http://dx.doi.org/10.5194/gi-4-149-2015.

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Abstract:

Abstract. The study of the deep structure of the Earth's crust is of great interest for both applied (e.g. mineral exploration) and scientific research. For this the electromagnetic (EM) studies which enable one to construct the distribution of electrical conductivity in the Earth's crust are of great use. The most common method of EM exploration is magnetotelluric sounding (MT). This passive method of research uses a wide range of natural geomagnetic variations as a powerful source of electromagnetic induction in the Earth, producing telluric current variations there. It includes the measurem

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50

Prystai, A. M., and V. O. Pronenko. "Improving of electrical channels for magnetotelluric sounding instrumentation." Geoscientific Instrumentation, Methods and Data Systems Discussions 5, no. 1 (2015): 63–81. http://dx.doi.org/10.5194/gid-5-63-2015.

Full text

Abstract:

Abstract. The study of deep structure of the Earth's crust is of great interest for both applied (e.g. mineral exploration) and scientific research. For this the electromagnetic (EM) studies which enable to construct the distribution of electrical conductivity in the Earth's crust are of great use. The most common method of EM exploration is magnetotelluric sounding (MT). This passive method of research uses a wide range of natural geomagnetic variations as a powerful source of electromagnetic induction in the Earth, producing there telluric currents variations. It includes the measurements of

APA, Harvard, Vancouver, ISO, and other styles

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